洛阳盆地地热资源形成条件与开发利用研究  

The Research on Formation Condition and Development of Geothermal Resources in LuoYang Basin

作　　者：王现国[1] 董永志[1] 杨现国[2] 杜春彦[3] 

机构地区：[1]河南省地矿局第二水文地质工程地质队,河南郑州450053 [2]河南省煤田地质局煤田地质勘察院,河南郑州450053 [3]河南省国土资源科学研究院,河南郑州450053

出　　处：《地下水》2007年第4期74-76,85,共4页Ground water

摘　　要：洛阳盆地地热田位于河南省西部,根据边山地热田和洛阳盆地近年来地热勘查情况,经对洛阳盆地地热背景及控热构造条件分析认为:洛阳盆地为NW向断裂(F1、F2)和NE向断裂(首阳山断裂、洛河断裂、伊河断裂F3)挟持的地热储存体。延伸并隐伏于洛阳盆地中的边山地热田控热构造F1、F2断层,仍具有导热、导水性质;F3、F41断层与F1、F2断层相交,被F1、F2错开,使F3、F41也具有导热、导水性。洛阳盆地热储层为下第三系砂、砾岩层,局部为∈3灰岩含水层。　The geothermal field in LuoYang basin lies in the west of HeNan province.According to the geothermal exploration of Bian-Shan geothermal field and LuoYang basin in the recent years,on the basis of analyzing the geothermal background and heat-controlled geologic structure condition of LuoYang basin,the paper concludes that the fracture of F1 and F2,which extend along northwest,and Shou-Yang Shan fracture,Luo-He fracture,Yi-He fracture,which extend along northeast,in LuoYang basin control the geothermal storage unit.The Bian-Shan geothermal field,which extends and lies concealed in LuoYang basin,controls the fracture F1 and F2,and has the heat and water conducting feature.The fracture F3 and F41 cut with fracture F1 and F2,and are staggered by F1 and F2,enabling fractures F3 and F41 also have the heat and water conducting function. The study shows that the geothermal storage unit in LuoYang basin consists of sand and gravel layers and some（∈3） limestone aquifer in the Tertiary.

关 键 词：洛阳地热田 地热资源 开发利用 

分 类 号：P314.1[天文地球—固体地球物理学]